Lenschow, 2005: Observations of drizzle in nocturnal marine stratocumulus
These water-needy locales all share certain physical requirements for converting fog to usable water for their populations: prevailing winds from a cool, offshore marine environment; elevated landforms at least thirteen hundred feet above sea level for maximum fog-water collection and within three to six miles of the coast, where fog-collecting arrays can be sited perpendicular to the onshore wind; recurring marine stratocumulus
clouds that intercept these land-forms and become fog; and the technical facilities and know-how to convert these life-giving fogs into potable water.
and cirrus clouds do not spawn thunderstorms, tornadoes or other severe weather, so they haven't attracted as much attention from researchers as more menacing cloud forms.
The purpose of this case was to investigate the accuracy and efficiency of these approaches in the context of drizzling stratocumulus
Heymsfield, 2007: Ice properties of single-layer stratocumulus
during the Mixed-Phase Arctic Cloud Experiment: 2.
So if exactly half of the sky is covered by stratus at 1000 feet with the rest covered by stratocumulus
at 2500 feet, the ceiling is 2500 feet because the stratus doesn't cover more than half of the sky, but the higher layer takes the total over half.
25) for a mixture of air from the top of a stratocumulus
cloud and air from just above the inversion.
University of Washington Controls on the Stratocumulus
In benign situations, "lake effect" clouds develop, consisting of stratus over the waters and shores, and stratocumulus
up to 50-100 nm inland.
Lin 2007) and erroneous stratocumulus
cloud cover, that play a crucial role in the climate response to external forcing.
When solar heating is not very strong, pilots may encounter the stratocumulus
Illingworth, 2005: Stratocumulus
liquid water content from dualwavelength radar.